首页> 外文期刊>Journal of vertebrate paleontology >FIRST SKULL OF ORTHASPIDOTHERIUM EDWARDSI (MAMMALIA, 'CONDYLARTHRA') FROM THE LATE PALEOCENE OF BERRU (FRANCE) AND PHYLOGENETIC AFFINITIES OF THE ENIGMATIC EUROPEAN FAMILY PLEURASPIDOTHERIIDAE
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FIRST SKULL OF ORTHASPIDOTHERIUM EDWARDSI (MAMMALIA, 'CONDYLARTHRA') FROM THE LATE PALEOCENE OF BERRU (FRANCE) AND PHYLOGENETIC AFFINITIES OF THE ENIGMATIC EUROPEAN FAMILY PLEURASPIDOTHERIIDAE

机译:柏鲁(法国)的晚新世和欧洲神秘家族的欧洲亲缘植物亲缘性的邻生爱德华氏菌(哺乳动物,“ CON突”)的第一个头骨

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摘要

Among the archaic 'ungulates,' pleuraspidotheriids are well documented by skulls and postcranial elements of Pleuraspidotherium from Berru and Cernay-les-Reims (late Paleocene, Paris Basin, France). Nevertheless, the relationships of pleuraspidotheriids (i.e., Pleuraspidotherium, Orthaspidotherium, and Hilalia) to other 'condylarths' have not been conclusively settled. They have been related to the typically North American Meniscotheriidae, Phenacodontidae, and Mioclaenidae, and even to the modern ungulates Perissodactyla and Artiodactyla. We here provide additional data, especially from the first complete skull of Orthaspidotherium, and highlight a mosaic of plesiomorphic and derived characters that distinguish Pleuraspidotheriidae from all other 'ungulates.' Their basicranial morphology approximates the ancestral morphotype of artiodactyls, but this results from symplesiomorphies. Pleuraspidotheriids exhibit the following synapomorphies: strong processes on the petrosal and enclosure of the facial nerve by the tympanic process and tympanohyal. Although their dentition resembles that of perissodactyls, meniscotheriids, and phenacodontids, the development of a pseudohypocone from the metaconule unambiguously shows that these similarities arose by convergence. Other evolutionary tendencies are the strong reduction of the hypoconulid, molarization of last premolars, development of lingual cingulum on M2, lengthening of the snout, and presence of diastemata. The pleuraspidotheriid tarsal morphology is primitive and not uncommon among 'condylarths' but presents some synapomorphies such as a calcaneum with a transverse cuboid facet and an astragalus with a squatting facet, cotylar fossa, and sustentacular hinge. Our study does not indicate a close relationship of Pleuraspidotheriidae with any of the archaic or modern 'ungulates' mentioned above. Instead, primitive arctocyonids could represent a possible ancestral morphotype for pleuraspidotheriids.
机译:在古老的“有蹄类动物”中,胸膜上的蛇颈兽有大量的文献记载,它们来自Berru和Cernay-les-Reims(古新世晚期,法国巴黎盆地)的胸膜上蛇骨的颅骨和颅后元素。然而,胸膜上皮动物(即胸膜上皮动物,角膜上皮动物和希尔拉利亚)与其他“ con”的关系尚未得到最终解决。它们与典型的北美门氏科(Meniscotheriidae),费氏科(Phenacodontidae)和M科(Mioclaenidae)有关,甚至与现代有蹄类动物Perissodactyla和Artiodactyla有关。我们在这里提供了其他数据,尤其是从Orthaspidotherium的第一个完整头骨中提取的数据,并突出显示了将Pleuraspidotheriidae与所有其他“有蹄类动物”区分开的多形和衍生字符的镶嵌图。它们的基本形态是近似于偶极动物的祖先形态,但这是由单纯形态引起的。胸膜胸膜突触表现出以下突触型:鼓膜过程和鼓膜引起的椎管和面部神经周围的强烈突触。尽管它们的齿列类似于过十二指,齿皮类和酚醛类,但从元锥中the假圆锥体的发育明确表明这些相似性是通过收敛而产生的。其他进化趋势是过度收缩,最后前磨牙的磨牙化,M2上舌状扣带的发育,口鼻部的延长和双性腺的存在。胸膜other骨的形态是原始的,在“ dy突”中并不罕见,但表现为一些突触,例如跟骨有横长方体小面,黄芪有蹲面,子叶窝和小结节。我们的研究没有表明翼le科与上述任何古老的或现代的“有蹄类动物”都有密切的关系。取而代之的是,原始的拱鼻龙可能代表了胸膜上鼻祖的可能的祖先形态型。

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